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Aurora australis (also known as the southern lights, and southern polar lights) is the southern hemisphere counterpart to the aurora borealis. In the sky, an aurora australis takes the shape of a curtain of light, or a sheet, or a diffuse glow; it most often is green, sometimes red, and occasionally other colors too. Aurora Australis over the elevated station at Amundsen-Scott South Pole Station, Antarctica.
The aurora borealis is also called the northern lights. The aurora borealis most often occurs from September to October and March to April. Its southern counterpart, aurora australis, has similar properties. The cause of the aurora is charged particles from the solar wind, accelerated by the Earth's magnetic field, colliding with atoms in the upper atmosphere causing them to glow as they release their surplus energy.